earthquake-the shaking of the Earth stress-force that changes a rock's formation shearing-stress that sends giant chunks of rock in opposite paths tension-stress that stretches rock so much that it causes the middle to become skinnier than before. compression-stress that pushes rock together until it folds or cracks deformation-physical change in the Earth's crust fault- crack in the Earth's crust where mounds of rock pass each other strike-slip fault-type of fault where rock on either side move past each other sideways with an up-or-down motion normal fault-the Hanging wall is faced downward, while the footwall is upward reverse fault-type of fault where the hanging wall comes upward hanging wall-upper half of fault footwall-forms lower half of fault fold-caused by bends in the part of Earth's crust when compression pushes the rock together anticline-causes the rock to bend upward,forming an arch syncline-a fold at the bottom of the rock,creating a "U" shaped structure plateau-flat land that is located high above sea level
Outline
Stress in the crust
Earthquake
shaking and trembling of the earth's surface
stress
force that changes rock's formation
Types of Stress
Shearing
causes rock to break or change formation
Tension
makes rock thin in the middle by stretching the rock
Compression
squeezes rock together until it folds or breaks
Deformation
change in volume or shape of the earth's crust
Kinds of Faults
shearing causes strike-slip faults
Strike-Slip Faults
fault where both sides of rock slip past each other with an up/down motion
tension causes normal faults
Normal Faults
fault where the hanging wall lies above the footwall
fault is at an angle
compression causes reverse faults
Reverse Fault
fault where footwall lies above the hanging wall
Friction Along Faults
friction
friction is a force that opposes one rock as it moves on another
Mountain building
plate movement can build up Earth's surface
Mountain Formed by Faulting
Fault Block Mountain
tension force makes lots of normal faults
when two normal faults are parallel,one block is in between
when block in between slides upward, a valley forms
Mountains Formed by Folding
Sometimes,plate movement causes crust to fold
when compression stresses rock,it can cause folding of the crust
Antyclines and Synclines
when compression has folded the rock,anticlines and synclines can be revealed
Plateaus
some are formed when verticle faults push up a flat block of rock
has lots of different layers,contains more width than height due to layers
Table of Contents
Earth's Crust in Motion
Vocabulary
earthquake-the shaking of the Earth
stress-force that changes a rock's formation
shearing-stress that sends giant chunks of rock in opposite paths
tension-stress that stretches rock so much that it causes the middle to become skinnier than before.
compression-stress that pushes rock together until it folds or cracks
deformation-physical change in the Earth's crust
fault- crack in the Earth's crust where mounds of rock pass each other
strike-slip fault-type of fault where rock on either side move past each other sideways with an up-or-down motion
normal fault-the Hanging wall is faced downward, while the footwall is upward
reverse fault-type of fault where the hanging wall comes upward
hanging wall-upper half of fault
footwall-forms lower half of fault
fold-caused by bends in the part of Earth's crust when compression pushes the rock together
anticline-causes the rock to bend upward,forming an arch
syncline-a fold at the bottom of the rock,creating a "U" shaped structure
plateau-flat land that is located high above sea level
Outline
Stress in the crust
Types of Stress
Kinds of Faults
Friction Along Faults
Mountain building
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